Matter, Energy, and Temperature
To understand the world of fundamental particles, we must first become familiar with the extreme scales on which nature operates – and with the way size, energy, and temperature are interconnected. That is the aim of this chapter.
Orders of magnitude and scales
An adult human is about 1.7 m tall – in scientific notation: the order of magnitude of m. That notation may sound abstract, but it is indispensable in physics. The universe spans a range of more than 44 orders of magnitude: from the smallest particles we know ( m) to the observable universe ( m). A single step in order of magnitude means a factor of ten.
To make such extremes manageable, physics uses adapted units:
- Ångström (Å) – m: the typical size of an atom.
- Fermi (fm) – m: the scale of an atomic nucleus.
- Light-year – m: the distance light travels in one year.
Within our solar system, Earth itself is m across, the Sun m, and Earth's orbit around the Sun m. Our galaxy measures m. Galaxies cluster into groups ( m) and superclusters ( m); the observable universe extends to m. Each step in that sequence represents at least a factor of ten to a hundred in distance.
At the atomic scale the ratio is even more extreme. An atom ( m) relates to its nucleus ( m) as a football stadium relates to a marble. Electrons and quarks are smaller than m – a ratio of 1 to 10,000 relative to the nucleus. An atom is therefore overwhelmingly empty space.
Energy at subatomic scales
On the human scale, we measure energy in joules. For subatomic particles, however, the joule is enormously inconvenient: an electron accelerated through a 1 V battery gains only J. Even in the world's most powerful accelerators, particles reach 'only' J – comparable to the kinetic energy of a fly.
Particle physics therefore uses its own unit: the electronvolt (eV):
For higher energies, familiar prefixes apply: keV ( eV), MeV ( eV), GeV ( eV), and TeV ( eV).
The electronvolt also connects energy to mass, through Einstein's . Because the speed of light is a fixed constant, every mass has a direct energy equivalent. A proton thus has a mass of 938.3 MeV/ and an electron 511 keV/. In practice, the is often dropped and physicists simply say 'a proton of 938 MeV'.
Temperature
Temperature is a macroscopic concept – not a property of a single particle, but a statistical average over a large ensemble of particles. The warmer a system, the greater the average kinetic energy with which its particles move and collide. This coupling is established by the Boltzmann constant ( eV/K): at room temperature ( K), the average kinetic energy per particle is about 0.025 eV – the thermal energy.
That number has direct physical meaning. When the thermal energy of colliding particles becomes comparable to a binding energy, a collision is energetic enough to break that bond. The binding energy of the outermost electron in a neutral atom is typically 1–10 eV, corresponding to temperatures of K. Below that threshold, atoms are stable; above it, they are ionised as collisions become energetic enough to knock electrons free.
The same reasoning applies at higher scales. In the core of the Sun ( K), the thermal energy is so large that no bound atom can survive. At K ( MeV), collisions are so violent that new particles can be created: two photons then carry enough energy to materialise an electron–positron pair. Above GeV, protons and antiprotons can spontaneously emerge from pure energy.
Energy, wavelength, and 'seeing' structure
How do we look at something? Light falls on it, reflects, and reaches our eyes. But visible light has a wavelength of 400–700 nm ( m) – a thousand times larger than an atom. To 'see' something, the wavelength of the radiation used must be smaller than the object being observed: the wavelength determines the resolving power (the resolution) of the observation. Atom-scale structure requires X-rays ( m, 10–100 keV). For nuclei and quarks, even shorter wavelengths – and therefore higher energies – are required.
Quantum mechanics tells us that the energy and wavelength of radiation are directly linked:
This is the central principle behind particle accelerators: the higher the energy, the smaller the structure we can probe.
This closes the triangle. The previous section linked temperature to energy (); this relation links energy to wavelength (). A system at temperature emits radiation with a characteristic wavelength . The three quantities – energy, wavelength, and temperature – are interchangeable.
The interactive explorer below shows seven characteristic energy scales – from the cosmic microwave background to the LHC frontier. Select a scale to read off the corresponding wavelength and temperature.
Select an energy scale. The probe peak shows which physical structures can be resolved at that energy – read off the corresponding wavelength and temperature in the axis label.
The table below brings those scales together:
| Energy | Wavelength | Temperature | Scale |
|---|---|---|---|
| 0.3 meV | ~4 mm | 3 K | Cosmic microwave background |
| 25 meV | ~50 µm | 300 K | Room temperature |
| 1 eV | ~1 µm | K | Atomic shell |
| 1 keV | ~1 nm | K | Solar core |
| 1 MeV | ~1 pm | K | Particle creation (electron) |
| 1 GeV | ~1 fm | K | Particle creation (proton) |
| 1 TeV | ~ m | K | LHC frontier |
When cosmologists speak of 'the universe at a temperature of K', they mean precisely this: the average energy per particle at that moment was ~1 MeV, with a corresponding wavelength of ~1 pm. At that energy scale, processes such as the creation of electron–positron pairs dominated – and that determined what the universe looked like in that phase. The table therefore translates not only laboratory physics into cosmology, but also the reverse: each step in temperature reveals a different layer of nature.